导水率
润湿
均方误差
毛细管作用
土壤水分
含水量
磁导率
土壤科学
相关系数
材料科学
岩土工程
数学
环境科学
地质学
化学
复合材料
统计
膜
生物化学
作者
Qiang Liu,Ping Xi,Guojun Liu,Jiali Miao,Fengzhu Liu
摘要
Abstract The unsaturated soil hydraulic conductivity function is one of the keys to solving unsaturated seepage issues. The wetting front advancing method (WFAM) is a proposed method for quickly measuring the coefficient of permeability of the unsaturated soils, but it has some demerits and limitations. In this study, a series of capillary rise tests were conducted and the coefficient of permeability of six kinds of unsaturated soils were obtained by using the WFAM. Based on the analyzing of characteristic changes in volumetric water content via soil moisture sensors in the capillary rise test, improvements were made to the method of determining the wetting front advancing velocity. The RMSE evaluation index was used to analyze the deviation of the data obtained by the improved method from the original visual method. The RMSE of the wetting front advancing velocity ranged from 0.0007 to 0.0074 cm s –1 , and the RMSE of the coefficient of permeability ranged from 0 to 5.2 × 10 –6 m s –1 . The results indicated the applicability of the improved method.
科研通智能强力驱动
Strongly Powered by AbleSci AI